
handle: 10272/13951
Clay mineralogy of the continetal and shallow marine sediments of Permian and Triassic age of the SE Iberian Ranges is a neglected subject. The present study shows the temporal variations of clay mineral assemblages and point out to two main primary controls: nature of the source area and sedimentary environments. Later diagenetic processes have not altered substantially the original mineralogy
Minerales de la arcilla, Paleogeografía, Triásico, Pérmico, Cordillera Ibérica SE
Minerales de la arcilla, Paleogeografía, Triásico, Pérmico, Cordillera Ibérica SE
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